thunderstorm and lightning rainfall and floodings
Some fancy names have been given to this question, Convectional, Orographic and Frontal. I will stick to the more simple types such as Lite falls , mediums falls and heavy or flooding rains. I am also including mist and fog because they both contain water vapour.
Equatorial regions experience convectional rainfall because of the intense heating of the sun, which warms the air near the surface. This warm air rises rapidly, cools, condenses, and forms clouds that lead to heavy rainfall. The constant heating and rising of warm, moist air in these regions create a cycle of convectional rainfall.
Convectional rainfall occurs around tropical islands and equatorial continents because the warm air heats the surface, causing it to rise rapidly and cool in the upper atmosphere. This rapid ascent of warm air leads to the condensation of water vapor and the formation of cumulus clouds, resulting in heavy rainfall.
Convectional rainfall occurs when the energy of the heats the earth’s surface and causes water to evaporate changing to water vapor which then forms clouds and rain comes down.
relief rainfall convectional rainfall Frontal rainfall
Convectional rainfall
because why not
thunderstorm and lightning rainfall and floodings
convectional rainfall
Some fancy names have been given to this question, Convectional, Orographic and Frontal. I will stick to the more simple types such as Lite falls , mediums falls and heavy or flooding rains. I am also including mist and fog because they both contain water vapour.
Equatorial regions experience convectional rainfall because of the intense heating of the sun, which warms the air near the surface. This warm air rises rapidly, cools, condenses, and forms clouds that lead to heavy rainfall. The constant heating and rising of warm, moist air in these regions create a cycle of convectional rainfall.
Convectional and orographic are types of rainfall. Convectional rainfall occurs when the ground is heated, causing warm air to rise and form cumulonimbus clouds that can result in localized heavy downpours. Orographic rainfall happens when moist air is forced to rise over mountain ranges, leading to cooling, condensation, and precipitation on the windward side of the mountains.
Convectional rainfall is when the sun heats the ground and hot air rises, the hot air then cools down and forms clouds then it rains
The three main types of rainfall are: convectional rainfall, relief rainfall and frontal rainfall. Relief rainfall is when the warm moist air from the sea ( Atlantic Ocean) is forced to rise over mountains and as the moist air gets higher it gets colder so it gradually condenses and becomes water droplets and it rains/ prcipitates. Relief rainfall is common along the west side of Britain where there are more high lands. Convectional rainfall is when the sun comes out and heats up the land, this causes the air around it to become warm too. The warm air currents rise and as it rises it gets colder so it gradually condenses and the water vapou become water droplets and it rains/precipitates. Convectional rainfall is mostly common around towards the south of Britain in the summer. Frontal rainfall is when cold air and warm air meet, the warm, light air wants to get past the heavy cold air so it casually rises above it. Its rising makes it get colder which makes the warm air cold air, so it condenses and becomes rain/ precipitation! Frontal rainfall is mostly common all over Britain especially in the winter.
Convectional rainfall occurs as a result of one of the three mechanisms that produce rain. When a fluid, such as air, is warmed from the bottom, for instance by earth warmed by sunlight, the lighter air rises drawing cooler air in underneath it. This sets up a so-called convectional flow. If the air near the ground is moist then when the it rises it will form clouds whose droplets coalesce to form convectional rain.
As the air rises, it cools and condenses. Clouds form and precipitation occurs.